Brea Mariana, Zucol Alejandro F
Laboratorio de Paleobotánica, Centro de Investigaciones Científicas, Diamante (CICYTTP-Diamante, CONICET), Matteri y España SN, E3105BWA Diamante, Entre Ríos, Argentina.
Ann Bot. 2007 Oct;100(4):711-23. doi: 10.1093/aob/mcm175. Epub 2007 Aug 29.
The anatomical characterization and morphology of Guadua zuloagae nov. sp. (Poaceae-Bambusoideae) culm was determined. This material was collected at the Toma Vieja fossil locality, Paraná basin, Argentina. This fossil culm is the first record of Bambusoideae in sediments of the Pliocene from the Ituzaingó Formation. The studied specimen was compared with the taxa of the Bambusoideae sub-family, especially with the American woody bamboos and others taxa that have woody culms, including Arundo, Thysalonaena and Gynerium.
The material was preserved by siliceous cellular permineralization, and it was prepared for microscopic examination by surface polishing and thin sections. The morphology and anatomy of this new species were described. The estimated height, critical buckling height and safety factor were calculated on the basis of the fossil bamboo diameter using the formula of Niklas. The relationship and comparison with the nearest living relatives (NLRs) are discussed.
Well-preserved petrified culm with internodes and nodes from the Pliocene of Argentina provides the basis for the description of a new fossil bamboo, Guadua zuloagae. The results of the anatomical analysis of the fossil bamboo showed a great affinity with the extant species Guadua angustifolia and constitute the first evidence of petrified bamboo culm.
The new fossil bamboo culm constitutes the only fossil record, preserved as permineralized by silicification, in the world. This fossil record indicates that the genus Guadua was more widespread in the past than today. Discovery of G. zuloagae allows the presence of a Bambusoideae understorey in the mixed forests described for the Ituzaingó Formation to be inferred. The climatic conditions inferred from fossil bamboo and sedimentary deposits indicate a temperate-warm, humid climate.
对新物种祖洛阿盖瓜多竹(Guadua zuloagae nov. sp.)(禾本科—竹亚科)的茎进行了解剖特征和形态学研究。该材料采自阿根廷巴拉那盆地的托马维耶哈化石地点。这种化石茎是竹亚科在伊图扎因戈组上新世沉积物中的首次记录。将研究标本与竹亚科的分类群进行了比较,特别是与美洲木本竹类以及其他具有木本茎的分类群,包括芦竹属(Arundo)、筒轴茅属(Thysalonaena)和大黍属(Gynerium)。
该材料通过硅质细胞全矿化保存,并通过表面抛光和薄片制备用于显微镜检查。描述了这个新物种的形态和解剖结构。根据化石竹茎的直径,使用尼克拉斯公式计算了估计高度、临界屈曲高度和安全系数。讨论了与最近现存近缘种(NLRs)的关系和比较。
来自阿根廷上新世保存完好的石化茎,带有节间和节,为描述一种新的化石竹——祖洛阿盖瓜多竹提供了依据。对该化石竹的解剖分析结果表明,它与现存物种狭叶瓜多竹(Guadua angustifolia)有很强的亲缘关系,并且构成了石化竹茎的首个证据。
这种新的化石竹茎是世界上唯一通过硅化全矿化保存下来的化石记录。这一化石记录表明,瓜多竹属在过去比现在分布更广。祖洛阿盖瓜多竹的发现使得可以推断出伊图扎因戈组所描述的混交林中存在竹亚科下层植被。从化石竹和沉积矿床推断出的气候条件表明当时是温暖湿润的温带气候。